Sequence striating and depositional environments of the Shamokin (Union Springs) Member, Marcellus Formation, and associated strata in the middle Appalachian Basin

Daniel Kohl, Rudy Slingerland, Michael Allan Arthur, Reed Bracht, James Terry Engelder

Research output: Contribution to journalArticle

31 Citations (Scopus)

Abstract

Organic-carbon-rich shales of the lower Marcellus Formation were deposited at the toe and basinward of a prograding clinothem associated with a Mahantango Formation delta complex centered near Harrisburg, Pennsylvania. Distribution of these organic-carbon-rich shales was influenced by shifts in the delta complex driven by changes in rates of accommodation creation and by a topographically high carbonate bank that formed along the Findlay-Algonquin arch during deposition of the Onondaga Formation. Specifically, we interpret the Union Springs member (Shamokin Member of the Marcellus For-mation) and the Onondaga Formation as comprising a single third-order depositional sequence. The Onondaga Formation was deposited in the lowstand to transgressive systems tract, and the Union Springs member was deposited in the trans-gressive, highstand, and falling-stage systems tract. The regional extent of parasequences, systems tracts, and the interpreted depositional sequence suggest that base-level fluctuations were primarily caused by allogenic forcing-eustasy, climate, or regional thermal uplift or subsidence-instead of basement fault reactivation as argued by previous workers. Paleowater depths in the region of Marcellus Formation black mudrock accumulation were at least 330 ft (100 m) as estimated by differences in strata thickness between the northwestern carbonate bank and basinal facies to the southeast. Geochemical analysis indicates anoxic to euxinic bottom-water conditions. These con-ditions were supported by a deep, stratified basin with a lack of circulation.

Original languageEnglish (US)
Pages (from-to)483-513
Number of pages31
JournalAAPG Bulletin
Volume98
Issue number3
DOIs
StatePublished - Jan 1 2014

Fingerprint

systems tract
Carbonates
Organic carbon
depositional environment
depositional sequence
Subsidence
Arches
organic carbon
basin
carbonate
parasequence
eustacy
lowstand
highstand
arch
reactivation
bottom water
mudstone
Water
subsidence

All Science Journal Classification (ASJC) codes

  • Fuel Technology
  • Energy Engineering and Power Technology
  • Geology
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)

Cite this

Kohl, Daniel ; Slingerland, Rudy ; Arthur, Michael Allan ; Bracht, Reed ; Engelder, James Terry. / Sequence striating and depositional environments of the Shamokin (Union Springs) Member, Marcellus Formation, and associated strata in the middle Appalachian Basin. In: AAPG Bulletin. 2014 ; Vol. 98, No. 3. pp. 483-513.
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Sequence striating and depositional environments of the Shamokin (Union Springs) Member, Marcellus Formation, and associated strata in the middle Appalachian Basin. / Kohl, Daniel; Slingerland, Rudy; Arthur, Michael Allan; Bracht, Reed; Engelder, James Terry.

In: AAPG Bulletin, Vol. 98, No. 3, 01.01.2014, p. 483-513.

Research output: Contribution to journalArticle

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